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Resolution of the age structure of the detrital zircon populations of two Lower Cretaceous sandstones from the Weald of England by fission track dating

Published online by Cambridge University Press:  01 May 2009

A. J. Hurford ,
F. J. Fitch  and
A. Clarke
A. J. Hurford
Affiliation:
Laboratory for Isotope Geology, University of Bern, Erlachstrasse 9a, 3012 Bern, Switerland
F. J. Fitch
Affiliation:
Department of Geology, Birkbeck College, University of London, 7/15 Gresse Street, London W1P 1PA
A. Clarke
Affiliation:
Department of Geology, Birkbeck College, University of London, 7/15 Gresse Street, London W1P 1PA
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Abstract

Modes in the frequency of distribution of fission track ages obtained from detrital zircon grains may prove characteristic of individual sandstone bodies, supporting the identification of the sources from which a particular flow of sedimentary detritus was derived and thus allowing new inferences to be made concerning palaeogeography. A computer program has been written and used to identify modes in the zircon fission track age distribution within two Lower Cretaceous sandstone samples from the Weald of southern England. Pronounced modes appear in one rock around 119 Ma, 160 Ma, 243 Ma and 309 Ma and in the other around 141 Ma, 175 Ma, 257 to 277 Ma and 394 to 453 Ma. The geological implications of these quite dissimilar zircon age spectra are discussed. It is concluded that they support the palaeogeographical models of Allen (1981) and indicate that the provenance of the first sample, from the Top Ashdown Sandstone member at Dallington in East Sussex, was almost entirely southerly, while that of the second, from the Netherside Sand member at Northchapel in West Sussex, was more varied, but predominantly westerly and northerly.

Type
Articles
Information
Geological Magazine , Volume 121 , Issue 4 , July 1984 , pp. 269 - 277
Copyright
Copyright © Cambridge University Press 1984

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